Multimodel projections of stratospheric ozone in the 21st century
By Veronika Eyring, D. Waugh, G. Bodeker, E. Cordero, H. Akiyoshi, J. Austin, S. Beagley, Byron A. Boville, P. Braesicke, C. Brühl and 30 more. 2007
335 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/c009460dab038c226b54cb5f7f0a21efdd717f47
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Citations in the corpus
- Aerosol and ozone changes as forcing for climate evolution between 1850 and 2100 (2013, background): “…emission evolution as well as climate change: PHOTOCOMP for tropospheric chemistry (Gauss et al. 2006; Stevenson et al. 2006; Dentener et al. 2006a), CCMVal for stratospheric ozone (Eyring et al. 2005, 2006, 2007; SPARC 2010) and AeroCom for aerosols (Kinne et al. 2006; Schulz et al. 2006).”
- Dynamics, stratospheric ozone, and climate change (2008, methodology): “(All these CMAM results are shown in Eyring et al. (2007) in the context of the other models.)”
- Retrieval of stratospheric temperatures from Atmospheric Infrared Sounder radiance measurements for gravity wave studies (2009, background): “…called gravity waves (or buoyancy waves) are generally unresolved or poorly resolved in most global models, yet they are known to have profound effects on the circulation, temperature structure, and chemistry of the middle atmosphere [Lindzen, 1973; Fritts and Alexander, 2003; Eyring et al., 2007].”
- Ozone hole and Southern Hemisphere climate change (2009, positive): “This asymmetry is consistent with the observed and predicted ozone trends [ Eyring et al. , 2007], i.e., a relatively rapid depletion followed by a slower recovery.”
- A Robust Mechanism for Strengthening of the Brewer–Dobson Circulation in Response to Climate Change: Critical-Layer Control of Subtropical Wave Breaking (2011, methodology): “For the calculations presented in this study, we use an ensemble of three 150-yr transient simulations starting in 1950, carried out as part of phase one of the Stratospheric Processes and their Role in Climate (SPARC) CCM Validation Activity (CCMVal-1) model intercomparison (Eyring et al. 2007).”
- Large climate-induced changes in ultraviolet index and stratosphere-to-troposphere ozone flux (2009, methodology): “To study the impact of climate change on the ozone layer requires stratosphere-resolving chemistry climate models (CCMs) with interactive stratospheric chemistr”